T 1.5 - 1.9 Flashcards

1
Q

Physical processes that volcanoes cause

A
  • lava flows
  • pyroclastic flows
  • ash falls
  • gas eruptions
  • secondary hazards - lahars, jökulhlaup
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2
Q

What are lava flows and how are they caused?

A
  • molten magma on the earths surface is so hot, it flows
  • viscosity determined by the amount of silicon dioxide
  • buildings can be burnt and covered if it is running
  • 1977: lake wall collapsed and lava drained in 1 hr, across 9km, swallowing villages while people were asleep
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3
Q

Gas steam emissions from volcanic eruptions:

A
  • h20 vapour: rainfall events, then potentially lahars
  • steam escapes though geysers
  • so2 forms very fine particles that get into the stratosphere, also causes acid rain which corrodes buildings and affects vegetation
  • fluorine gas is poisonous in high conc. and contaminated farmland or water supply
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4
Q

What are pyroclastic flows and how are they caused?

A
  • frothing bubbles of molten magma in the vent, burst explosively to eject a dense mixture of hot gases and pyroclastic material, eg glass, pumice, ash
  • can reach temperatures of up to a 1000
  • move rapidly down side of volcano up to 700km/h
  • leave behind volcanic deposits ( can dam rivers)
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5
Q

How are ash falls caused and what are they?

A
  • carried into the atmosphere, potentially even trans boundary
  • most fall locally, causing roofs to collapse, breathing difficulties for people and animals, bury crops
  • disrupts flights paths of planes
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6
Q

How are lahars caused and what are they?

A
  • water mixed with volcanic deposits, flowing rapidly along existing valleys
  • could be caused by heavy rain, or maybe volcanic ash has has created humid air, condensation, clouds and rain
  • very fast (60kmh) carry large amounts of material
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7
Q

Impacts of Mountain Nyiracongo eruption

A
  • major eruptions in 1977, 2002, 2021
  • 2km wide continuous lava lake
  • responsible for 40% of Africa’s volcanic eruptions
  • shield volcano
    2002 - 147 killed, 400k evacuated
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8
Q

Eykafjallajokull eruption 2010

A
  • single eruption divided into many phases
  • 14th April, relatively explosive eruption (4 on VEI)
  • situated 200m under glacial ice, where melt water caused two things: rapidly vaporising water, rapid lava cooling created cloud of abrasive glass rich ash
  • but deaths = 0
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9
Q

Social/ human impacts of Eykafjallajokull eruption

A
  • cancelled sports, music and arts events
  • localised health effects around south Iceland due to abrasive ash
  • increased regional traffic for land based travel
  • cancelled/postponed political events
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10
Q

Economic impacts of eykafjallajokull eruption

A
  • European economy lost 5 billion
  • African economies lost as much as 65 million
  • loss for airlines ($1.1 billion)
  • knock on effect from cancelled events (eg, MotoGP in Japan)
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11
Q

Regional significance of eykafjallajokull eruption

A
  • ash cloud reached as far as northern Italy, meaning any flights to and from Europe were affected
  • increased in land based travel so train prices and road traffic rose
  • however reduced air and noise pollution recorded around Europe
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12
Q

Global significance of eykafjallajokull eruption

A
  • Japan MotoGP suffering
  • Kenyan flower industry lost 2 million
  • New Zealand fish farmers still were winners as they could have more domestic demand
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13
Q

Land use zoning

A
  • keeping residential and commercial zones away from active dormant volcanoes
  • easier with shield volcanoes
  • hard because of soi fertility
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14
Q

Hazard resistant design

A
  • retrofit buildings
  • cross bracing
    but this is expensive on a national scale and requires government legislation
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15
Q

Engineering defences

A
  • sea walls and mangroves to absorb wave energy
  • back up utility plans for hospitals and police stations
  • drain craters to prevent lahars
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16
Q

Diversion of lava flows

A
  • spray sea water to solidify lava and create basalt rock to diverse lava flows
17
Q

Remote sensing

A
  • monitor gas emissions
  • cloud monitoring
  • monitor fault line staring
  • tilitometers measure ground deformation
18
Q

Hawaii earthquake facts and figures

A
  • early may 2018
  • magnitude 6.9
  • 24 fissures
  • 2000 people evacuated, with damage to electricity generation
  • $800m damage
19
Q

How they become disasters - local variables

A
  • distance from source (waves lose energy longer you go)
  • offshore bathymetry (shallow or deep)
  • coastal topography and geology
  • extent vertical fault displacement
20
Q

Benioff zone

A
  • area with height seismic activity/ slab moving downward
  • speed and movement of rock produces earthquake
  • locked faults are significant concern
  • slab builds tension due to frictional resistance, until they release a huge amount of energy in the form of an earthquake
21
Q

How tectonics could affect landslides

A
  • focal depth (changes MMS)
  • change amounts of folding (steeper)
  • change lava type
  • hydration melting - more explosive andesitic lava
22
Q

Stresses at a plate boundary

A
  • angle of slope
  • rainwater/ saturation
  • vibration
  • earthquakes
  • sea/cliff erosion
23
Q

Strengths at a plate boundary

A
  • lubricant layers
  • tree vegetation roots
  • consolidation of material
  • porosity of soil
24
Q

Chile - The Andes 🇨🇱

A
  • convergent plate boundary
  • Anzac plate below the South American plate
  • major EQ and volcanic eruptions
  • EQ can trigger avalanches, rock avalanches and landslides
25
Q

Punta Cola avalanche:

A

Strength - tree bunds land together giving it resistance

Stress - water doing hydraulic action breaking the land cashing a landslide

26
Q

Characteristics of a shield volcano

A
  • constructive plate boundary
  • divergence
  • lower silicates and gas content in magma
  • continuous eruption
  • runny, basaltic lava, gentle slope, shorter volcano
27
Q

Characteristics of a composite volcano

A
  • destructive plate boundary
  • subduction
  • higher silicates and gas content in magma
  • longer dormancy, pressure build up
  • explosive eruption, gas and material
  • viscous andesitic lava
  • steep sided tall volcano
28
Q

So overall, how are landslides formed at destructive plate boundary?

A
  • one plate is folded up
  • steeper gradient
  • increased gravity in this plate which can increase likelihood of landslides
  • magma can melt the plate = landslides
29
Q

1.8 overall

A

Tsunamis form and are shaped by coastal morphology e.g Indian Ocean

30
Q

Keychain for tsunami

A

• Destructive plate boundary
• Subduction zone
• Earthquake
• Megathrust fault – water displacement
• Wave… which is fine until the sea-bed shelves
• Then friction drags at the bottom of wave as bed shelves
• Wave frequency / amplitude changes and grows before hitting land
• Backwash out, swash in (wave crash)